It is emphasized that the first flooding surface (FFS) is used as a standard or useful marker in optimizing chronostratigraphic and lithostratigraphic boundaries.
在地层方面,进一步强调以初始海泛面(FFS)作为优化地层“阶”的准。
It is emphasized that the first flooding surface (FFS) is used as a standard or useful marker in optimizing chronostratigraphic and lithostratigraphic boundaries.
在地层方面,进一步强调以初始海泛面(FFS)作为优化地层“阶”的准。
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